TY - JOUR
T1 - Real-Space Renormalization Estimates for Two-Phase Flow in Porous Media
AU - Hansen, Alex
AU - Roux, Stéphane
AU - Aharony, Amnon
AU - Feder, Jens
AU - Jøssang, Torstein
AU - Hardy, H. H.
PY - 1997
Y1 - 1997
N2 - We present a spatial renormalization group algorithm to handle immiscible two-phase flow in heterogeneous porous media. We call this algorithm FRACTAM-R, where FRACTAM is an acronym for Fast Renormalization Algorithm for Correlated Transport in Anisotropic Media, and the R stands for relative permeability. Originally, FRACTAM was an approximate iterative process that replaces the L x L lattice of grid blocks, representing the reservoir, by a (L/2) x (L/2) one. In fact, FRACTAM replaces the original L x L lattice by a hierarchical (fractal) lattice, in such a way that finding the solution of the two-phase flow equations becomes trivial. This triviality translates in practice into computer efficiency. For N = L x L grid blocks we find that the computer time necessary to calculate fractional flow F(t) and pressure P(t) as a function of time scales as τ ∼ N1.7 for FRACTAM-R. This should be contrasted with the computational time of a conventional grid simulator τ ∼ N2.3. The solution we find in this way is an acurate approximation to the direct solution of the original problem.
AB - We present a spatial renormalization group algorithm to handle immiscible two-phase flow in heterogeneous porous media. We call this algorithm FRACTAM-R, where FRACTAM is an acronym for Fast Renormalization Algorithm for Correlated Transport in Anisotropic Media, and the R stands for relative permeability. Originally, FRACTAM was an approximate iterative process that replaces the L x L lattice of grid blocks, representing the reservoir, by a (L/2) x (L/2) one. In fact, FRACTAM replaces the original L x L lattice by a hierarchical (fractal) lattice, in such a way that finding the solution of the two-phase flow equations becomes trivial. This triviality translates in practice into computer efficiency. For N = L x L grid blocks we find that the computer time necessary to calculate fractional flow F(t) and pressure P(t) as a function of time scales as τ ∼ N1.7 for FRACTAM-R. This should be contrasted with the computational time of a conventional grid simulator τ ∼ N2.3. The solution we find in this way is an acurate approximation to the direct solution of the original problem.
KW - Effective properties
KW - Heterogeneity
KW - Relative permeability
KW - Renormalization numerical algorithm
KW - Simulation
UR - http://www.scopus.com/inward/record.url?scp=0031430142&partnerID=8YFLogxK
U2 - 10.1023/A:1006593820928
DO - 10.1023/A:1006593820928
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AN - SCOPUS:0031430142
SN - 0169-3913
VL - 29
SP - 247
EP - 279
JO - Transport in Porous Media
JF - Transport in Porous Media
IS - 3
ER -